Abstract

Theory and observation tell us that many complex systems exhibit tipping points—thresholds involving an abrupt and irreversible transition to a contrasting dynamical regime. Such events are commonly referred to as critical transitions. Current research seeks to develop early warning signals (EWS) of critical transitions that could help prevent undesirable events such as ecosystem collapse. However, conventional EWS do not indicate the type of transition, since they are based on the generic phenomena of critical slowing down. For instance, they may fail to distinguish the onset of oscillations (e.g. Hopf bifurcation) from a transition to a distant attractor (e.g. Fold bifurcation). Moreover, conventional EWS are less reliable in systems with density-dependent noise. Other EWS based on the power spectrum (spectral EWS) have been proposed, but they rely upon spectral reddening, which does not occur prior to critical transitions with an oscillatory component. Here, we use Ornstein–Uhlenbeck theory to derive analytic approximations for EWS prior to each type of local bifurcation, thereby creating new spectral EWS that provide greater sensitivity to transition proximity; higher robustness to density-dependent noise and bifurcation type; and clues to the type of approaching transition. We demonstrate the advantage of applying these spectral EWS in concert with conventional EWS using a population model, and show that they provide a characteristic signal prior to two different Hopf bifurcations in data from a predator–prey chemostat experiment. The ability to better infer and differentiate the nature of upcoming transitions in complex systems will help humanity manage critical transitions in the Anthropocene Era.

Highlights

  • The understanding that complex systems can possess thresholds marking a sudden shift to an alternative dynamical regime has been around for a long time

  • A significant development in this area is that of early warning signals (EWS), which are a suite of statistical metrics that are expected to undergo observable change prior to a tipping point [5,6]

  • Most EWS are grounded in the phenomenon of ‘critical slowing down’, which is a generic feature of local bifurcations [7]

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Summary

Introduction

The understanding that complex systems can possess thresholds marking a sudden shift to an alternative dynamical regime has been around for a long time (e.g. in ecology [1,2]) Such a threshold may be referred to directly as a tipping point/ catastrophic bifurcation, or by its inferred dynamics, a critical transition/regime shift. Most EWS are grounded in the phenomenon of ‘critical slowing down’, which is a generic feature of local bifurcations [7] It involves the degradation of restoring forces along some dimension of the system’s state space, resulting in a longer return time to equilibrium following a perturbation. We use the term ‘conventional EWS’ to refer to these EWS that serve as proxies for critical slowing down

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